Search results
Results From The WOW.Com Content Network
As the lava flowed across the wet sod, the water of the marsh started to boil, the vapour rising through the lava forming lava pillars from drainpipe size up to several meters in diameter. [4] As the lava continued flowing towards lower ground in the Mývatn area, the top crust collapsed, but the hollow pillars of solidified lava remained. The ...
The word lava comes from Italian and is probably derived from the Latin word labes, which means a fall or slide. [2] [3] An early use of the word in connection with extrusion of magma from below the surface is found in a short account of the 1737 eruption of Vesuvius, written by Francesco Serao, who described "a flow of fiery lava" as an analogy to the flow of water and mud down the flanks of ...
Formed of basanite, it is a remnant of a basaltic lake formed of solidified lava and is the site of the most recent volcanic activity in the range. It was formed 2.9 million years ago, above an accumulation of several layers of pyroclastic trachyandesite .
Pele's tears (closest Hawaiian translation: "nā waimaka o Pele") are small pieces of solidified lava drops formed when airborne particles of molten material fuse into tearlike drops of volcanic glass. Pele's tears are jet black in color and are often found on one end of a strand of Pele's hair.
The erupting lava met the water of the Indian Ocean during the August 2004 eruption. Video of a lava flow in August 2019 2004 eruption Animated map of eruptions between 1972 and 2000. Most eruptions of Piton de la Fournaise are of the Hawaiian style: fluid basaltic lava flowing out with
A solidified lava pond that consists of a massive gray basalt with weakly developed columnar jointing occupies the crater of Vulcan. Radial, sinuous lava tubes 8 to 20 inches (200 to 510 mm) across and 300 feet (91 m) long are preserved on the northeast and northwest flanks of Vulcan. [2] [3]
These caves were formed around 890,000 years ago from a volcanic eruption in Paul da Serra that ran down to the sea. Thus, the outside, exposed to lower temperatures solidified rapidly while the inner liquid continued to run with many gases, forming a series of lava tubes, which today constitute the caves of São Vicente.
Collapse of the frontal part of lava deltas is common during their formation, representing a hazard for any people that are watching from a solidified part of the delta and such areas are normally marked as dangerous. [8] If a newly formed lava bench rests on sediments, it may pose hazards due to its extremely unstable structure. [6]